- Hydrology and Sediment Transport Processes
- Hydrology and Watershed Management Studies
- Soil erosion and sediment transport
- Iterative Methods for Nonlinear Equations
- Advanced Optimization Algorithms Research
- Flood Risk Assessment and Management
- Matrix Theory and Algorithms
- Hydraulic flow and structures
- Coastal wetland ecosystem dynamics
- Fractional Differential Equations Solutions
- Coastal and Marine Dynamics
- Geological formations and processes
- Environmental and Agricultural Sciences
- Environmental Changes in China
- Fish Ecology and Management Studies
- Water Quality Monitoring Technologies
- Coastal and Marine Management
- Groundwater flow and contamination studies
- Hydrological Forecasting Using AI
- Climate variability and models
- Radioactive element chemistry and processing
- Fluid Dynamics and Vibration Analysis
- Wastewater Treatment and Nitrogen Removal
- Chaos control and synchronization
- Geochemistry and Geologic Mapping
Wuhan University
2015-2024
Harbin Institute of Technology
2020-2023
Henan Institute of Geological Survey
2023
State Key Laboratory of Water Resources and Hydropower Engineering Science
2009-2022
Central South University
2022
Anhui University of Technology
2022
Tianjin University
2022
Tsinghua University
2021
University Town of Shenzhen
2021
Wayne State University
2021
The sediment budget is a method to study the distribution of in different parts river basin. This paper studies Yangtze River by analyzing data on soil erosion, size distributions deposits, load, and fluvial process. A determine for proposed which total erosion from upstream reaches tributaries divided into two parts: load transported Yichang station storage gullies. Furthermore, three bed material deposited middle lower process, wash estuary, deposition Tongting Lake. estuary further very...
Abstract Understanding the effects of climate variability and reservoir operation on runoff is important for shipping, irrigation water supply services, especially during extreme drought years. After Three Gorges Dam (TGD) began, discharge processes in mid-lower reaches Yangtze River were completely different from those pre-dam period. The measured hydrological data Mike 11-HD model used to estimate contributions TGD variation results are as follows: under drought, special phenomenon a...
Abstract Understanding the mechanisms controlling downstream water‐level variations after operation of Three Gorges Dam is important for riverine flood and drought management. However, our quantitative understanding multiple controls river morphology, vegetation, floodplain resistance on water levels in Middle Yangtze River (MYR) remains limited. Here, we analyze changes channels MYR using 450 cross‐sectional profiles as well data discharge, levels, sediment, satellite images from 2003 to...
Alluvial fans develop at the base of mountain fronts, where rivers emerge from constrained area onto plain. Acting as a transition zone between streams and alluvial rivers, fan-river system is typically characterized by slope break in bed profile, significant discontinuity surface sediment fining gravel-sized to sand-sized, sudden increase channel width. In large with great morphological diversity strong human interference, shift upstream downstream river morphology dynamics within exhibits...
Abstract Dunes are important for bedload transport in almost all large river systems and exert an control flow resistance. Investigating dunes is fundamental simulating discharge, sediment transport, flood routing. However, the spatiotemporal dynamics of resistance remain poorly understood alluvial mainly due to lack high‐resolution data. Here we analyzed in‐field observed data on annual profiles 450 cross‐sections, bathymetry, water levels, Middle Yangtze River, found that developed...
Abstract Damming profoundly affects downstream flow‐sediment regimes, altering channel bar dynamics and thereby affecting floods riverine biodiversity. Here, we investigate the response of bars to upstream damming by examining patterns, mechanisms, impacts in Middle Yangtze River (∼1,000 km). Over a decade post‐damming observational data reveal substantial increases revegetation Leaf Area Index. Shorter flood duration stable size collectively drive greening. Consequently, denser vegetation...